“…Besides these two indicator species, we observed additional taxa that are highly abundant in the burnt samples, including Vulcaniibacterium (Gammaproteobacteria, Xanthomonadaceae), Escherichia-Shigella (Gammaproteobacteria, Enterobacteriaceae), Pseudomonas (Gammaproteobacteria, Pseudomonadaceae), Methylobacterium-Methylorubrum (Alphaproteobacteria, Rhizobiales), Aeribacillus (Bacilli, Bacillaceae), Romboutsia (Clostridia, Peptostreptococcaceae), Paraclostridium (Clostridia, Peptostreptococcaceae) and Clos-tridium_sensu_stricto_1 (Clostridia, Clostridiaceae). Some of these taxa have been frequently reported to be associated with decomposing remains and carcasses (i.e., Pseudomonadaceae, Xanthomonadaceae, Enterobacteriaceae [1,44,49,[86][87][88]). Vulcaniibacterium, similarly to Pyrinomonas, has been isolated from a geothermally heated soil samples [88], and their presence in charred samples is therefore not completely unexpected.…”